{"refrec":{"BRefID":6051,"RR":"<b>Orford, J.D.; Wilson, P.; Wintle, A.G.; Knight, J.; Braley, S.</b> (2000). Holocene coastal dune initiation in Northumberland and Norfolk, eastern UK: climate and sea-level changes as possible forcing agents for dune initiation, <b><i>in</i></b>: Shennan, I. <i>et al.</i> <i>Holocene land-ocean interaction and environmental change around the North Sea. Geological Society Special Publication,</i> 166: pp. 197-217. <a href=\"https://dx.doi.org/10.1144/GSL.SP.2000.166.01.11\" target=\"_blank\">https://dx.doi.org/10.1144/GSL.SP.2000.166.01.11</a>","BEntID":6051,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Shennan, I. <i>et al.</i> <i>Holocene land-ocean interaction and environmental change around the North Sea. Geological Society Special Publication,</i> 166: pp. 197-217. <a href=\"https://dx.doi.org/10.1144/GSL.SP.2000.166.01.11\" target=\"_blank\">https://dx.doi.org/10.1144/GSL.SP.2000.166.01.11</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Orford, J.D.; Wilson, P.; Wintle, A.G.; Knight, J.; Braley, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Orford, J.D. <i>et al.</i>","Englishabstract":"Relative sea-level (RSL) control on dune initiation during the Holocene is examined in the context of chronostratigraphies established from 43 vibracores through dunes and into sub-dune sediments taken from the Northumberland and Norfolk (UK) coasts. The chronology is based on 23 accelerated mass spectroscopy and conventional 14C dates, and 37 infra-red-stimulated luminescence dates. The oldest dunes in Northumberland are c. 4 cal. ka BP with phases of dune development at 2.8 and 1.5–1 ka BP. Most dune deposition is of last millennium age, with a concentration, especially in Norfolk, around 500–200 a BP. The initiation...","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"Holocene coastal dune initiation in Northumberland and Norfolk, eastern UK: climate and sea-level changes as possible forcing agents for dune initiation","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2000,"MonPub":null,"DateUpdate":"2022-03-22","DateCreate":"2001-02-09","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1144/GSL.SP.2000.166.01.11"},"refs":null,"anarec":{"AnaID":6051,"PubliDate":2000,"Pagination":"197-217","XtraPublOfAnaID":null,"ISBN":"1-86239-054-1","Volume":"166","Issue":null,"BRefMon":5963,"BRefMonRR":"<b>Shennan, I.; Andrews, J. (Ed.)</b> (2000). 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